沉积盆地地温梯度研究中应注意的问题

沉积盆地的地温场特征是油气勘探研究的重要内容之一。油气勘探工作者习惯于采用地温梯度而不是大地热流来描述沉积盆地的热状态,但是,地温梯度与计算井段密切相关,离开计算井段去谈地温梯度高低,很容易引起误解,尤其是在测温井段较短或测温深度较浅时,测温数据不能直接用于计算沉积盆地的地温梯度,否则,会得出错误的结论。然而,在实际研究工作中,这一点经常被忽视。为此,本文提出了“规一化”地温梯度的概念和计算方法,并以实例说明沉积盆地地温场研究中,采用“规一化”地温梯度来描述盆地热状态平面分布特征的必要性。     

Shaking table test and numerical analysis of a 1：12 scale model of a special concentrically braced steel frame with pinned connections

<正>This paper describes shaking table tests of a 1:12 scale model of a special concentrically braced steel frame with pinned connections,which was fabricated according to a one-bay braced frame selected from a typical main factory building of a large thermal power plant.In order to investigate the seismic performance of this type of structure,several ground motion accelerations with different levels for seismic intensityⅧ,based on the Chinese Code for Seismic Design of Buildings,were selected to excite the model.The results show that the design methods of the members and the connections are adequate and that the structural system will perform well in regions of high seismicity.In addition to the tests,numerical simulations were also conducted and the results showed good agreement with the test results.Thus,the numerical model is shown to be accurate and the beam element can be used to model this structural system.     

中国近海异常海温数值预报模式研究Ⅰ.模式的建立

本文从近海异常海温的定义和形成机制出发,在原有的海表温度数值预报模式的基础上,考虑了上层海洋对强天气强迫的动力响应和浅海效应,前者包括卷入和卷出、冷水抽吸和暖水辐聚,后者包括潮混合和浅海对短波吸收之影响,从而建立了一个以混合层的温、流、深度为变量的中国近海异常海温数值预报模式.     

Analyses of factors forming offshore SST anomaly(O-SSTA) in China seas

INTRoDUCTIONThestatusofChinaseasisverycomplicated.First,itisoftendisturbedbystrongsynopticsy8tems,suchastheadvanceandretreatofthesubtropichighs,theactivityofthetyphoonsandthecoldwavesetc;next,ithascomplexwater-systemswhicharecontrolledbyaplanetary-scalecurrentsyStemofKuroshio;inaddition,italsohasacomplicatedtopographyandwidecontinen-talshelves(about4OOkmwide).Underthesecircumstances,theSSTvariesObviouslythrough-outtheyear.OneoutstandingvariationistheoffshoreSSTanomaly,namely,crSSTA.…     

A PRELIMINARY STUDY ON MEANFIELD DECOMPOSITION

Two kinds of the empirical orthogonal function analysis method for decomposing the mean-field are developed and a comparison is made between them. It is proved that the mean-field can be decomposed using eigenvectors obtained from anomaly-field decomposition, and that more information can be obtained. An example of sea bottom mean temperature analysis shows its remarhabk effect in depicting the distribution features of variousfactors, such as cold water mass, currents and radiation.A few problems concerning the efficiency of the method are discussedand two matrices of relationship which represent the space-time characteristics of the field are derived. The formulae of space-time transformation are obtained conveniently.     

Application of method of fuzzy sets to the analysis of water masses in the northern South China Sea

Some methods of fuzzy sels are applied to the analysis of water masses in the north area of the South China Sea. In distinguishing water masses with the fuzzy clustering method, the authors propose a fuzzy similar relation based on Euclidean distance, and suggest a method for determining the number of water masses by the F-test, and further adjust rationally the boundaries of water masses and the membership relation of samples by the elastic classification method. Eight water masses are distinguished in the area, i.e., Nearshore Diluted Water F, Nearshore Mixed Water M, Warm Surface Water WS, Surface Water S, Surface-Subsurface Mixed Water SU, Subsurface Water U, Subsurface-Intermediate Mixed Water UI and Intermediate Water I. These point-sets of various water masseson the (?)-S diagram may be summed up in three types, that is, the deformed elliptical convexpoint-set, the half-boundless convex point-set and the point-set with single-side concave. For them, we have proposed methods of making their member     

Water masses in the northern South China Sea

Using the fuzzy clustering as the principal method, eight water masses in the northern South China Sea (NSCS) are distinguished. They are Alongshore Diluted Water Mass (F), Nearshore Mixed Water Mass (M), Warm Surface Water Mass(WS), Surface Water Mass(S), Surface-Subsurface Mixed Water Mass(SU), Subsurface Water Mass (U), Subsurface-Intermediate Water Mass (UI) and Intermediate Water Mass (1). A synthertic study is made on the formations, basic properties and modified characters of each water mass and the regularities of their disributions and growth and decline variations . They may be classified into three types; the type of runoff-diluted water (F). the type of shallow sea-modified water (M, WS. S. and SU) and the type of deep sea-oceanic water (U, UI, and I).     

A numerical forecasting model of offshore-SST anomaly

INTRODUCTIONTheO-SSTAisdefinedas:theSSTanomalyinoffshoreisover2twiththehorizontalscopeofover1"longitudemultipliedbyl'latitudeandthetime-scalesofover10d.ItisanoutstandingoceanographicphenomenonoccurringagainandagainintheChinaseasinallseasons.TheaffectingfactorsoftheO-SSTAhavebeendiscussedindetail,whichincludebothoftheresponseofupperoceantothestrongatmosphericsystemsandtheshallow-watereffects(Wangetal.,1998).HoweverthereisnoexplorationhowadynamicpredictingmodelofO-SSTAisdeveloped.Th…     

模糊数学方法在南海北部海区水团分析中的应用

Some methods of fuzzy sets are applied to the analysis of water masses in the north area of the South China Sea. In distinguishing water masses with the fuzzy clustering method, the authors propose a fuzzy similar relation based on Euclidean distance, and suggest a method for determining the number of water masses by the F-test, and further adjust rationally the boundaries of water masses and the membership relation of samples by the elastic classification method. Eight water masses are distinguished in the area, i.e., Nearshore Diluted Water F, Nearshore Mixed Water M, Warm Surface Water WS, Surface Water S, Surface-Subsurface Mixed Water SU, Subsurface Water U, Subsurface- Intermediate Mixed Water UI and Intermediate Water I. These point-sets of various water masses on the θ-S diagram may be summed up in three types, that is, the deformed elliptical convex point-set, the half-boundless convex point-set and the point-set with single-side concave. For them, we have proposed methods of making their memb     

A STUDY ON METHOD FOR EMPIRICAL ORTHOGONAL FIELD PREDICTION CONSIDERING INFLUENCE FACTORS

Sinee the predietion equations for EOF(Entpirical Orthogonal Fune-494青岛海洋大学学报1 9 89年tion)methods《belonging to 6eld foreeasting)are generally eonstrueted onthe basis of statistieal relations among predietands without eongidering theinnuenee of external faetors,while the regression analysis methods(晚long-ing to single·station foreeasting)eonsidering sueh in口uenee faeto“eannot show the internal relations among the predietand.〔l一3几The Pr暇ntPaper attemPts to introduee the innue…